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Titlebook: Ice Physics and the Natural Environment; John S. Wettlaufer,J. Gregory Dash,Norbert Unterst Conference proceedings 1999 Springer-Verlag Be

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发表于 2025-3-21 17:13:41 | 显示全部楼层 |阅读模式
书目名称Ice Physics and the Natural Environment
编辑John S. Wettlaufer,J. Gregory Dash,Norbert Unterst
视频video
概述A multidisciplinary treatise of the subject.Provides both up-to-date assessments for experts in the field and broad overviews for non-specialists
丛书名称Nato ASI Subseries I:
图书封面Titlebook: Ice Physics and the Natural Environment;  John S. Wettlaufer,J. Gregory Dash,Norbert Unterst Conference proceedings 1999 Springer-Verlag Be
描述The Advanced Study Institute Ice Physics in the Natural and Endangered Environ­ ment was held at Acquafredda di Maratea, Italy, from September 7 to 19, 1997. The ASI was designed to study the broad range of ice science and technology, and it brought together an appropriately interdisciplinary group of lecturers and students to study the many facets of the subject. The talks and poster presentations explored how basic molecular physics of ice have important environmental consequences, and, con­ versely, how natural phenomena present new questions for fundamental study. The of lectures discusses these linkages, in order that overall unity of following sunimary the subject and this volume can be perceived. Not all of the lecturers and participants were able to contribute a written piece, but their active involvement was crucial to the success of the Institute and thereby influenced the content of the volume. We began the Institute by retracing the history of the search for a microscopic un­ derstanding of melting. Our motivation was straightforward. Nearly every phenome­ non involving ice in the environment is influenced by the change of phase from solid to liquid or vice-versa. Hence
出版日期Conference proceedings 1999
关键词Cloud; Frost; Ocean; Oceanography; Scale; Sea ice; Snow; Storm; Thunder; Troposphere; Umwelt; environment; geoph
版次1
doihttps://doi.org/10.1007/978-3-642-60030-2
isbn_softcover978-3-642-64226-5
isbn_ebook978-3-642-60030-2Series ISSN 1431-7125
issn_series 1431-7125
copyrightSpringer-Verlag Berlin Heidelberg 1999
The information of publication is updating

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发表于 2025-3-21 20:22:58 | 显示全部楼层
History of the Search for a Theory of Melting quantum mechanics, concepts of long range order, the role of dimensionality in condensed matter, and more sensitive experimental techniques to test the theories. After years of probing the mechanism within the bulk material, we have discovered that the answer has been lying on the surface.
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Crystal Growth, Surface Phase Transitions and Thermomolecular Pressureerns how microscopic processes influence macroscopic behavior. Recent advances in understanding the surface phase transitions that alter the equilibrium and near equilibrium interfacial structure are central to many pattern formation problems during ice crystal growth, the geometric evolution of pol
发表于 2025-3-22 08:51:49 | 显示全部楼层
Some Aspects of the Physics of Glaciersmass conservation; the temperature distribution by considering heat sources and heat transfer by conduction and advection. The mechanisms of surging and of the tidewater-glacier instability are outlined. The interpretation of Heinrich Events as evidence of surges of the Laurentide Ice Sheet is criti
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Present and Past Glaciations: A Geological Perspectivey Palaeozoic (about 450 Ma), probably also the Late Proterozoic (Vendian: about 600 Ma) glaciations, affected large continents in high latitude south polar position. Asynchronous glaciation affected the southern and the northern continents during the Cenozoic. In Antarctica, it started during Eocene
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Ice in the Troposphere large in-cloud electric fields that give rise to lightning. These roles depend on the numbers, shapes, sizes, surface properties and spatial distributions of the particles. In this paper we discuss current understanding of the important processes involving tropospheric ice particles, with particula
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Physico-Chemistry of Polar Stratospheric Cloudsfusion-controlled bulk reactions on/in the particles, convert halogens, which derive from compounds of mainly anthropogenic origin, from relatively inert reservoir species into forms that efficiently destroy ozone. The microphysics of these particles under cold stratospheric conditions is still unce
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A Minimal Model of Sea Ice and Climatehe climate to increased concentration of greenhouse gases, the predicted amplification of climatic warming in the arctic, the possibility of multiple equilibria, and the waiting times between transitions from one equilibrium to another.
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